温度势的英文

• potential, temperature

• "温度"英文翻译    temperature
• "势"英文翻译    power; force; influence
• "审度势" 英文翻译 :    size uthe situation
• "湿度势" 英文翻译 :    moisture potential
• "速度势" 英文翻译 :    speed potential; velocity potential
• "等速度势面" 英文翻译 :    equipotential surface of velocity
• "等速度势线" 英文翻译 :    equipotential curve of velocity
• "定常速度势" 英文翻译 :    steady velocity potential
• "复数速度势" 英文翻译 :    complex velocity potential
• "复速度势" 英文翻译 :    complex velocity potential
• "加速度势" 英文翻译 :    acceleration potential
• "空间速度势" 英文翻译 :    spatial velocity potential
• "流势 ，速度势" 英文翻译 :    velocity potential
• "审时度势" 英文翻译 :    judge the hour and size up the situation; adopt a wait-and-see attitude; await the proper moment (to ...); observe the times and judge the occasion; see how matters stand; see how the gander hops; see how the land lies; make a correct assessment of the situation; correctly appraise the situation
• "速度势函数" 英文翻译 :    velocity potential function
• "速度势能" 英文翻译 :    velocity potential
• "速度势位" 英文翻译 :    velocity potential
• "非定常速度势" 英文翻译 :    unsteady velocity potential
• "下洗速度势法" 英文翻译 :    downwash-velocity potential method
• "温度" 英文翻译 :    [物理学] temperature 绝对温度 absolute temperature; 室内温度 indoor temperature; 室外温度 outdoor temperature; 最低温度 minimum temperature; 最高温度 maximum temperature; 温度标 scale of thermometer; 温度表 thermometer; thermograph; 温度差 temperature difference; 温度异常 temperature anomaly
• "比温度" 英文翻译 :    specific humidity
• "壁温度" 英文翻译 :    wall temperature
• "冰温度" 英文翻译 :    ice temperature
• "初温度" 英文翻译 :    beginning temperature
• "床温度" 英文翻译 :    bed temperature

• ( 5 ) based on 1 - d horizontal tests for coupled movement of soil water , salt and heat transfer , theoretical analyses on the influence of temperature gradient on soil water and salt movement were conducted
  西安理工大学博士学位论文（ 5 ）根据水平一维土壤水盐热耦合迁移试验，分析了温度势梯度对水盐运动影响的机理。
• The results indicate that soil water moves from the warm end to the cool end in both gaseous and aqueous phases under temperature gradient , which causes changes of matric po
  研究表明，在温度势梯度影响下土壤水分以液态和汽态两种状态从暖端向冷端迁移，从而引起暖端基质势的相应改变，导致水分在两种势梯度交互作用下逐渐达到平衡。
• Seepage influences on the temperature distribution by means of heat transfer and communication , temperature influences on seepage field by changing the hydraulic conductivity and inducing fluid flow because of the temperature potential , thus finally approaching the stable seepage and temperature fields
  渗流通过参与热量传递与交换影响温度分布，温度通过改变介质渗透系数和温度势梯度引起水流运动来影响渗流场，两者相互作用最终达到稳定的渗流场和温度场。